Christoffel Symbols
On a curved manifold there is no free lunch in differentiation. The partial derivative of a vector field compares components living in two different tangent spaces — the space at your foot and the space one step ahead — and those spaces are tilted relative to one another, so the naive difference is not a geometric object at all. To differentiate meaningfully you must supply extra structure that says how to carry a vector from one point to the next: a connection. The Christoffel symbols are the components of that connection in a coordinate basis. They record the rate at which the coordinate basis vectors tip and stretch as you slide an infinitesimal step, and thereby upgrade the flat partial derivative into the covariant derivative that respects the geometry. A general affine connection carries arbitrary data — its components are free functions. Riemannian geometry pins down one connection out of that infinitude by two physical demands. Metric compatibility, , keeps lengths and angles constant under transport, so a ruler stays a ruler as it moves. Vanishing torsion, , makes infinitesimal parallelograms close. The fundamental theorem of Riemannian geometry says these two conditions fix the connection uniquely, and the resulting coefficients — the Christoffel symbols, or Levi-Civita connection coefficients — are built entirely from first derivatives of the metric. This article takes those two conditions, owned by the metric-compatibility and torsion articles, and solves them for the one object that drives every concrete computation in general relativity: the geodesics that free particles follow, the parallel transport that measures holonomy, and, through their derivatives, the Riemann curvature that no coordinate choice can erase.
- The Christoffel symbols are the connection coefficients of the unique torsion-free, metric-compatible (Levi-Civita) connection — the bookkeeping for how basis vectors change point to point.
- They are fixed entirely by first derivatives of the metric: .
- They are NOT tensor components: a coordinate change adds an inhomogeneous second-derivative term, so they can be made to vanish at any single point — the local inertial frame of the equivalence principle.
- They are symmetric in the lower pair, , precisely because the connection is torsion-free.
- They drive the covariant derivative, the geodesic equation, and parallel transport, and — through and — assemble the Riemann curvature tensor.
- Key idea: demand that differentiation respect the metric (lengths preserved) and be symmetric (zero torsion); those two requirements uniquely solve for the connection coefficients in terms of metric derivatives — the Christoffel symbols.
Demand that differentiation respect the metric (lengths preserved) and be symmetric (zero torsion); these two requirements uniquely solve for the connection coefficients in terms of metric derivatives, yielding the Christoffel symbols.
Where this lives today
Every numerical relativity code that models a black-hole merger begins by computing Christoffel symbols. When LIGO and Virgo detect a gravitational wave, the template bank it is matched against comes from simulations that integrate Einstein's equations on a grid, and at each of billions of grid points the machine evaluates from the numerically evolved metric before assembling the Ricci and Einstein tensors. The same symbols drive the ray-tracing behind the Event Horizon Telescope's images of M87 and Sgr A: a photon's path through the warped spacetime around a black hole is a null geodesic, integrated through , and the bright ring you see is where those geodesics pile up near the photon sphere. Closer to home, the atomic clocks aboard GPS satellites are corrected for a gravitational redshift that is, at leading order, the of the weak-field metric integrated over the orbit — get the Christoffel symbol wrong and positions drift by kilometers per day. The frontier open problem is that the metric connection is torsion-free by fiat: theories with torsion (Einstein–Cartan gravity, and the teleparallel reformulations where curvature is traded for torsion entirely) keep the antisymmetric part that the Levi-Civita choice discards, and whether nature uses it is an experimental question still open at the interface of gravity and spin.
The physical picture
Draw a coordinate grid on a curved surface — lines of latitude and longitude on a globe, or circles and rays on a flat sheet of polar graph paper. The basis vectors and literally point in different directions and carry different lengths at different points: at the rim of a circle is longer than near the center, because a step of one radian in sweeps a longer arc when is large. The Christoffel symbols are the precise ledger of that tipping and rescaling. They answer the question, "if I pick up a basis vector here and slide it one infinitesimal step, how much has it turned and grown, so that I can subtract off that spurious change and isolate the real change in a vector field?" This is why nonzero does not by itself mean gravity. Flat two-dimensional space in polar coordinates has and — perfectly nonzero — yet the Riemann tensor vanishes everywhere. The symbols are recording the curvilinear grid, not any curvature of the space. The first figure makes this concrete: the basis vectors fan and stretch across a flat polar sheet, and the symbols quantify exactly that.
Now think of the equivalence principle. In a freely falling elevator, physics looks special-relativistic and gravity vanishes — no ball drops, no floor pushes up. Mathematically that freely falling observer can always choose coordinates in which at their location and the metric equals there. This is possible precisely because is not a tensor: a genuine tensor that is zero in one frame is zero in all, but the inhomogeneous piece in the transformation law can be dialed to cancel the symbols at one chosen point. What cannot be dialed away is the second derivative of the metric — the tidal stretching that pulls two nearby free-fall trajectories together or apart. That irreducible content lives in the derivatives , which assemble the Riemann tensor. Gravity is not the ; gravity is the part of that survives every coordinate choice.
Two routes give the same symbols. One grinds the metric formula with its three derivative terms and an inverse-metric contraction; the other writes the geodesic Lagrangian , runs the Euler–Lagrange equations, and reads the off as the coefficients of the velocity products. The second is far faster by hand and automatically respects the lower-index symmetry, which is why it is the working physicist's method.
The core equations
The master formula is the solution of the fundamental theorem: metric compatibility plus zero torsion, solved for the connection. Everything downstream — geodesics, transport, curvature — is a use of this one expression, so it is worth committing to memory in the form below, with its telltale pattern of two "plus" derivatives and one "minus".
where: — connection coefficient (Christoffel symbol of the second kind); — metric components; — inverse metric, ; — coordinate partial derivative. Physically: the symbol is a weighted gradient of the metric — it is nonzero exactly when the metric components vary from point to point, whether from genuine curvature or merely from a curvilinear grid. The symbols exist to fix differentiation. On a contravariant vector they add a correction with a plus sign; on a covariant one-form the correction flips sign, so that the derivative of a scalar stays an honest partial derivative and the two corrections cancel.
where: — contravariant vector components; — one-form components; — covariant derivative, whose output is a genuine tensor. Physically: measures the change of components including the spurious change of the basis; the term subtracts the basis change, leaving the true change of the vector. A geodesic is a curve that parallel-transports its own tangent — the straightest possible worldline. Setting the covariant derivative of the tangent along itself to zero gives the equation every free particle and light ray obeys.
where: — affine parameter (proper time for timelike geodesics); — the worldline. Physically: the term is the entire "gravitational force" in this picture — it is what bends a straight line in coordinates into a falling trajectory, and it can be transformed away locally because gravity is geometry, not a Newtonian force. The non-tensorial character is not a blemish but the source of the equivalence principle. Under a coordinate change the symbols transform with the usual homogeneous tensor piece plus an inhomogeneous term built from the second derivative of the coordinate map.
where: — new coordinates; the final term carries second derivatives of the map. Physically: because that extra term depends only on the coordinate change and not on any field value, it can be tuned to cancel at a chosen point — the mathematics of a freely falling frame. The antisymmetric-in-lower-indices part, however, is the genuine torsion tensor and transforms cleanly.
where: — torsion tensor, set to zero for the Levi-Civita connection. Physically: the vanishing of torsion is exactly the statement that infinitesimal coordinate parallelograms close, and it is what makes the lower index pair symmetric. Tracing one upper against one lower index collapses the three-term formula to a compact logarithmic derivative of the metric determinant — the single most useful identity for divergences and volume elements.
where: — metric determinant. Physically: this turns the covariant divergence into , the form used to write conservation laws and the invariant volume in curved spacetime. Finally, differentiating and squaring the symbols builds the object that no coordinate choice can remove — the Riemann curvature tensor, the true seat of gravity.
where: — Riemann curvature tensor, a genuine tensor although assembled from non-tensorial . Physically: the pieces are the tidal content that survives in a local inertial frame, and the pieces restore tensor character to the whole.
The goal is to prove the fundamental theorem of Riemannian geometry constructively: that metric compatibility and vanishing torsion, imposed together, do not merely constrain the connection but fix it completely, with the metric formula (1) as the explicit and unique solution. We start from , write it three times with the indices cyclically permuted, add two of them and subtract the third so the compatibility terms combine, use torsion-freedom to collapse the connection terms into a single factor, and finally raise the free index with the inverse metric. The three-permutation trick is the workhorse the reader should internalize.
Step 1. Write metric compatibility out in full, , so the partial derivative of the metric is expressed through the connection. Why: this converts the geometric condition into an algebraic relation among and that can be manipulated index by index.
Step 2. Reproduce the same equation twice more with indices cycled, , then add the first two and subtract the third to form . Why: the cyclic sum is engineered so that the four connection terms with mismatched index orders cancel in pairs, leaving only the symmetric combination we want.
Step 3. Apply zero torsion, , so the surviving terms merge into . Why: without symmetry the antisymmetric part of would remain undetermined — this is exactly where torsion-freedom does its work, killing the freedom that a general affine connection retains.
Step 4. Contract both sides with the inverse metric to free the upper index, giving , which is formula (1). Why: every component is now written explicitly in terms of the metric, so the solution exists and is unique — there is no residual freedom, proving the theorem. *Verified: reproduces MTW Eq. (8.24) and Wald Eq. (3.1.30); matches Carroll Eq. (3.27).*
Go deeper · Derivation B · 1 minChristoffel symbols from the geodesic Lagrangian
The goal is to establish the fast practical route that every working relativist uses instead of grinding formula (1): extract the symbols by varying the kinetic Lagrangian and reading them off as the coefficients of the velocity products in the resulting geodesic equations. This method sidesteps the explicit inverse-metric contraction, handles diagonal metrics almost instantly, and cannot accidentally break the lower-index symmetry, because the velocities enter symmetrically by construction. We derive the geodesic equation from the Euler–Lagrange equations and match.
Step 1. Take the Lagrangian with and affine parameter ; extremizing its integral yields the geodesic. Why: the kinetic form is the squared line element, so its stationary curves are exactly the straightest worldlines, and depends on the metric whose derivatives will surface as .
Step 2. Form the Euler–Lagrange equation with and . Why: these two partials are all the variational calculus needs, and the term is precisely the metric gradient that becomes a Christoffel symbol.
Step 3. Differentiate along the curve to get , then symmetrize the middle term over into . Why: the velocity product is symmetric, so only the symmetric part of its coefficient contributes — this is what regenerates the three-term structure of formula (1).
Step 4. Raise the index with to obtain ; the coefficient of is exactly . Why: in practice one never raises the index abstractly — one writes out the Euler–Lagrange equation for each coordinate and simply reads the symbols off the velocity terms, which is dramatically faster than summing formula (1). *Verified: equivalent to the metric formula; standard in Hartle §8.4 and Schutz §6.5.*
Go deeper · Derivation C · 1 minVanishing at a point and the local inertial frame
The goal is to prove the geometric content of the equivalence principle: that at any chosen point there exist coordinates in which every Christoffel symbol vanishes, so a freely falling observer sees no gravity locally, while the curvature encoded in stubbornly remains. The proof uses the inhomogeneous transformation law (4) directly — we expand the coordinate change to second order about , keep a free quadratic coefficient, and choose it to exactly cancel the symbols at . The construction works only because is symmetric in its lower indices, tying this result back to zero torsion.
Step 1. Expand the new-to-old coordinate map about as , with , the linear part set to the identity, and a free coefficient symmetric in . Why: the identity linear part keeps the metric orthonormal at , while the quadratic term is the only new freedom that can influence at .
Step 2. Evaluate the second-derivative block, , and note the first-derivative Jacobian is at . Why: these are precisely the two objects the transformation law (4) needs, and evaluating at makes the Jacobians trivial so the law simplifies.
Step 3. Insert into the transformation law (4) to get . Why: with unit Jacobians the homogeneous term is just the old symbol and the inhomogeneous term is just , so the new symbol is their sum — a quantity we can now zero out by choice.
Step 4. Choose , which is a legal choice because both sides are symmetric in ; then . Why: the symmetry of (from zero torsion) is exactly what makes a consistent quadratic coefficient — one cannot cancel an antisymmetric part this way. One can additionally set , but the second derivatives , i.e. the Riemann tensor, cannot be removed. *Verified: standard construction in MTW §11.6 and Carroll §3.3; relies on the lower-index symmetry of .*
Limiting cases
| Case | Result | Meaning |
|---|---|---|
| Flat space, Cartesian coordinates | Constant metric has zero derivatives, so every symbol vanishes and . | |
| Flat space, polar coordinates | Nonzero with zero curvature — the symbols track the curvilinear grid, not gravity. | |
| Diagonal metric | (no sum on ) | The inverse-metric contraction collapses to one term, so hand computation is fast. |
| Local inertial / Riemann normal at | Symbols vanish but their derivatives — the irreducible curvature — do not. | |
| Weak static field, slow particle | The geodesic equation reduces to , recovering Newtonian gravity from . |
Worked examples
1 · Christoffel symbols of the two-sphere (confidence builder)
The round two-sphere of radius has metric . Find all nonzero Christoffel symbols by the Lagrangian method, and evaluate them at colatitude .
Step 1. Write the Lagrangian and vary . The Euler–Lagrange equation gives , i.e. . Matching to reads off .
Step 2. Vary : expands to , i.e. . The factor of 2 splits between the two orderings and , giving . All other symbols vanish.
Step 3. Notice the radius has dropped out entirely — the symbols are scale-free, a direct sign that they encode angular geometry, not size. Evaluate at : and . At the 45° parallel, and , independent of the sphere's radius.
Step 4. Sanity check against the metric formula (1): , matching Step 1 exactly. These same symbols, differentiated once, give and hence the Gaussian curvature — the sphere is genuinely curved, unlike the flat polar sheet whose symbols also looked nonzero.
2 · Schwarzschild and the Newtonian limit (fully numeric)
The Schwarzschild metric in geometric units () is with . Compute , form the radial geodesic equation for a slowly moving particle, and evaluate at the surface of the Earth.
Step 1. With the metric diagonal, use the collapsed formula: . Since , this gives .
Step 2. The radial geodesic equation for a particle moving slowly () keeps only the term: . For weak fields we have and , so . Restoring units (, ) turns this into — Newton's law of gravity falls straight out of a Christoffel symbol.
Step 3. Plug in the Earth: and give — the surface gravity, reproduced to three figures. The relativistic correction factor is , utterly negligible, which is why Newtonian gravity is superb at the Earth's surface and the full is needed only near compact objects.
Step 4. Contrast the regimes: at the Earth's surface the correction is a part in ; at the Sun's photosphere , still tiny but enough to bend starlight measurably; at the Schwarzschild radius the factor makes vanish in these coordinates — a coordinate artifact of the horizon, not a physical fact, exactly the kind of -based illusion the misconception warning cautions against. Earth: , relativistic correction .
Physics of the portrait
The Christoffel symbols carry the name of a mathematician who never thought about gravity at all. They emerged from a purely geometric question — when are two quadratic differential forms equivalent under a change of variables — and only decades later became the language in which Einstein wrote the gravitational field.
Origins · 1 minElwin Bruno Christoffel and how this was discovered
Elwin Bruno Christoffel was a German mathematician, born in Montjoie (today Monschau) in 1829, who spent his most productive years at the newly founded Kaiser-Wilhelm-Universität in Strasbourg. In an 1869 paper in Crelle's Journal, "Über die Transformation der homogenen Differentialausdrücke zweiten Grades," he attacked the equivalence problem for quadratic differential forms — essentially, when can one metric be turned into another by a coordinate change. To answer it he introduced the symbols now bearing his name (of the first and second kind), the operation now called covariant differentiation, and, by iterating it, the four-index object now called the Riemann–Christoffel curvature tensor. Christoffel worked in the tradition of Riemann and Gauss and saw none of the physics ahead: his symbols were tools of pure differential geometry. Their destiny was fixed a generation later when Gregorio Ricci-Curbastro and his student Tullio Levi-Civita built the "absolute differential calculus" — tensor calculus — on exactly Christoffel's foundation, and when Einstein, guided by his friend Marcel Grossmann to that calculus, made the symbols the components of the gravitational field in the 1915 theory of general relativity. Levi-Civita's 1917 notion of parallel transport finally gave the symbols their intuitive geometric meaning as the rule for carrying a vector without turning it. Christoffel also worked in conformal mapping (the Schwarz–Christoffel transformation) and potential theory, but it is these connection coefficients — a bookkeeping device for curvature — that made his name a fixture of every relativity textbook.
Going further
Texts. Misner, Thorne & Wheeler, Gravitation, §8.5, §10.3, §13.4 · Wald, General Relativity, §3.1 · Carroll, Spacetime and Geometry, §3.1–3.3 · Schutz, A First Course in General Relativity, §5.3–5.6 · Hartle, Gravity, §8.4 and the appendix on the geodesic Lagrangian.
Provenance. The two defining conditions are recalled by name from the prerequisite articles — metric compatibility from aq-gr-metric-compatibility and vanishing torsion from aq-gr-torsion-tensor — and the general notion of a connection from aq-gr-affine-connection and aq-gr-covariant-derivative. All equations here are standard textbook results. A verifier should: (1) reproduce the metric formula (1) against MTW Eq. (8.24), Wald (3.1.30), Carroll (3.27); (2) confirm the flat-space polar values , from ; (3) verify the two-sphere values , and their evaluations and ; (4) check the Schwarzschild and its Earth-surface Newtonian limit with correction ; (5) confirm the contracted identity (6) via Jacobi's formula and the Riemann formula (7) against Carroll (3.112).
Prerequisites. The Affine Connection · Covariant Derivative · Metric Compatibility · Torsion Tensor. Leads to. The Levi-Civita Connection · The Geodesic Equation · Geodesics as Extremal Paths · Geodesic Deviation Equation · Parallel Transport.
Ask the tutor: Ask me to grind the Christoffel symbols of any metric you like — Schwarzschild, FRW, or a surface of your choosing — and watch the geodesic Lagrangian method beat the brute-force formula step by step.
Are Christoffel symbols the components of a tensor?
No, and this is their most important structural feature. Under a coordinate change they pick up an inhomogeneous term, , on top of the usual homogeneous tensor transformation. That extra piece depends only on the coordinate map, not on any field value, which is exactly why the symbols can be made to vanish at a chosen point even in curved spacetime. A genuine tensor cannot do this: if it is zero in one frame it is zero in all. Two useful corollaries: the difference of two connections is a tensor (the inhomogeneous terms cancel), and so is the antisymmetric part of a single connection — that is the torsion.
Why does the metric formula have two plus signs and one minus?
The pattern comes straight from the cyclic-permutation derivation. Metric compatibility written three times, with indices cycled, produces three copies of ; adding two of them and subtracting the third is the specific combination that makes the unwanted connection terms cancel and leaves a single symmetric . The surviving derivatives are : the two "plus" terms differentiate along the lower index directions and , and the "minus" term differentiates along the summed direction . It is not an arbitrary sign convention — swap it and the result no longer satisfies . Memorizing the pattern "two along the free lower indices, minus one along the dummy" is the quickest way to recall formula (1) correctly.
If nonzero Γ does not mean curvature, what does?
The Riemann tensor, , and nothing less. Curvature lives in the derivatives of the connection, not in the connection itself, which is why it can be nonzero even where the symbols vanish (Riemann normal coordinates) and zero even where they are large (flat space in polar coordinates). Operationally, curvature is what you measure by parallel-transporting a vector around a small closed loop: it comes back rotated by an amount proportional to times the enclosed area. On a sphere the rotation equals the enclosed solid angle; in flat space, whatever coordinates you use, it is exactly zero.
What is the difference between first-kind and second-kind Christoffel symbols?
The second-kind symbol has one raised index and is the object that appears in the covariant derivative and geodesic equation — it is what physicists almost always mean by "the Christoffel symbols." The first-kind symbol is the fully lowered version, , sometimes written in older texts. The two carry the same information; you raise or lower the first index with the metric. Both are symmetric in the last two indices. The only practical hazard is reading a formula from a source without checking which convention it uses, since a stray metric factor separates them.
How do I compute Christoffel symbols quickly by hand?
Use the geodesic Lagrangian, not the metric formula. Write with the explicit metric components, then write out the Euler–Lagrange equation for each coordinate. Each equation comes out in the form , and the coefficients are the Christoffel symbols directly — with the standard caveat that a cross term like splits equally between the two orderings, so . This method avoids inverting and summing over the metric, respects the lower-index symmetry automatically, and for a diagonal metric is several times faster than formula (1). Always cross-check one symbol against the metric formula the first time you use a new metric.
Why can gravity be transformed away locally but not globally?
Because a coordinate change has enough freedom to cancel the connection at a single point but not its derivatives everywhere. At a chosen point you can pick the quadratic part of the coordinate map to set every and the linear part to set — a freely falling frame in which physics looks special-relativistic. But the second derivatives , which combine into the Riemann tensor, involve independent higher coefficients of the map that the same choice cannot control. Physically, a uniform gravitational field is pure and can be erased by falling; a real field varies from place to place, and that variation — the tidal force pulling your head and feet apart, or two dropped balls together — is curvature, invariant under every coordinate choice. Local flatness is exact; global flatness would require .